Upper tropospheric conditions in relation to the cloud top features of 15 August 2010 convective storms

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F13%3A10130587" target="_blank" >RIV/00216208:11320/13:10130587 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68378289:_____/13:00394685 RIV/00020699:_____/13:#0000744 RIV/00216224:14310/13:00067515

Výsledek na webu

<a href="http://www.sciencedirect.com/science/article/pii/S0169809512003328" target="_blank" >http://www.sciencedirect.com/science/article/pii/S0169809512003328</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.atmosres.2012.10.006" target="_blank" >10.1016/j.atmosres.2012.10.006</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Upper tropospheric conditions in relation to the cloud top features of 15 August 2010 convective storms

Popis výsledku v původním jazyce

This study focuses on 15 August 2010, when many severe convective storms occurred over parts of central and Eastern Europe, with some of these exhibiting various interesting cloudtop characteristics observed by weather satellites. The importance of the phenomena of cold-U and cold-ring features in the infrared brightness temperature enhanced imagery stems from the fact that storms exhibiting these features are very often accompanied by severe weather. Therefore, besides the general description of the atmospheric conditions in the area, we seek possible reasons for the different cloud-top appearance of these storms from the perspective of Meteosat Second Generation and polar-orbiting weather satellites. Two main issues are discussed in this paper - theunusually warm appearance of the cloud-top of the "Prague hailstorm" and the presence of cold-ring and cold-U shaped storms in close proximity to the warmer "Prague hailstorm". Both of these issues prove that the storm top appearance is v

Název v anglickém jazyce

Upper tropospheric conditions in relation to the cloud top features of 15 August 2010 convective storms

Popis výsledku anglicky

This study focuses on 15 August 2010, when many severe convective storms occurred over parts of central and Eastern Europe, with some of these exhibiting various interesting cloudtop characteristics observed by weather satellites. The importance of the phenomena of cold-U and cold-ring features in the infrared brightness temperature enhanced imagery stems from the fact that storms exhibiting these features are very often accompanied by severe weather. Therefore, besides the general description of the atmospheric conditions in the area, we seek possible reasons for the different cloud-top appearance of these storms from the perspective of Meteosat Second Generation and polar-orbiting weather satellites. Two main issues are discussed in this paper - theunusually warm appearance of the cloud-top of the "Prague hailstorm" and the presence of cold-ring and cold-U shaped storms in close proximity to the warmer "Prague hailstorm". Both of these issues prove that the storm top appearance is v

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DG - Vědy o atmosféře, meteorologie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2013

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Atmospheric Research

ISSN

0169-8095

e-ISSN

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Svazek periodika

Neuveden

Číslo periodika v rámci svazku

123

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

19

Strana od-do

249-267

Kód UT WoS článku

000316580600020

EID výsledku v databázi Scopus

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